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First discovery of high-mercury silver in ores of the Rogovik gold–silver deposit (Northeastern Russia). / Makshakov, A. S.; Kravtsova, R. G.; Goryachev, N. A. и др.

в: Doklady Earth Sciences, Том 476, № 1, 01.09.2017, стр. 1094-1098.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Makshakov, AS, Kravtsova, RG, Goryachev, NA, Pal’yanova, GA & Pavlova, LA 2017, 'First discovery of high-mercury silver in ores of the Rogovik gold–silver deposit (Northeastern Russia)', Doklady Earth Sciences, Том. 476, № 1, стр. 1094-1098. https://doi.org/10.1134/S1028334X17090276

APA

Makshakov, A. S., Kravtsova, R. G., Goryachev, N. A., Pal’yanova, G. A., & Pavlova, L. A. (2017). First discovery of high-mercury silver in ores of the Rogovik gold–silver deposit (Northeastern Russia). Doklady Earth Sciences, 476(1), 1094-1098. https://doi.org/10.1134/S1028334X17090276

Vancouver

Makshakov AS, Kravtsova RG, Goryachev NA, Pal’yanova GA, Pavlova LA. First discovery of high-mercury silver in ores of the Rogovik gold–silver deposit (Northeastern Russia). Doklady Earth Sciences. 2017 сент. 1;476(1):1094-1098. doi: 10.1134/S1028334X17090276

Author

Makshakov, A. S. ; Kravtsova, R. G. ; Goryachev, N. A. и др. / First discovery of high-mercury silver in ores of the Rogovik gold–silver deposit (Northeastern Russia). в: Doklady Earth Sciences. 2017 ; Том 476, № 1. стр. 1094-1098.

BibTeX

@article{1397694f475842b9976490398559da6c,
title = "First discovery of high-mercury silver in ores of the Rogovik gold–silver deposit (Northeastern Russia)",
abstract = "New data on mercurial mineralization are presented, and a detailed characteristic is given for the first discovery of mercurous silver in ores of the Rogovik gold–silver deposit (the Omsukchan trough, Northeastern Russia). It was found that native silver in the examined ores occurs as finely-dispersed inclusions in quartz filling microcracks and interstitions. It also occurs in associations with kustelite, Ag sulfosalts and selenides, selenitic acanthite, and argyrodite. The mercury admixture varies from “not detected” in the central parts of grains to 0.22–1.70 wt % along the edges, or, in independent grains, to the appearance of Ag amalgams containing 10.20–24.61 wt % of Hg. The xenomorph form of grains of 50 μm or less in size prevails. It is assumed that the appearance of mercurial mineralization is caused by the superposition of products of the young Hg-bearing Dogda–Erikit belt upon the more ancient Ag-bearing Omsukchan trough.",
author = "Makshakov, {A. S.} and Kravtsova, {R. G.} and Goryachev, {N. A.} and Pal{\textquoteright}yanova, {G. A.} and Pavlova, {L. A.}",
year = "2017",
month = sep,
day = "1",
doi = "10.1134/S1028334X17090276",
language = "English",
volume = "476",
pages = "1094--1098",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "1",

}

RIS

TY - JOUR

T1 - First discovery of high-mercury silver in ores of the Rogovik gold–silver deposit (Northeastern Russia)

AU - Makshakov, A. S.

AU - Kravtsova, R. G.

AU - Goryachev, N. A.

AU - Pal’yanova, G. A.

AU - Pavlova, L. A.

PY - 2017/9/1

Y1 - 2017/9/1

N2 - New data on mercurial mineralization are presented, and a detailed characteristic is given for the first discovery of mercurous silver in ores of the Rogovik gold–silver deposit (the Omsukchan trough, Northeastern Russia). It was found that native silver in the examined ores occurs as finely-dispersed inclusions in quartz filling microcracks and interstitions. It also occurs in associations with kustelite, Ag sulfosalts and selenides, selenitic acanthite, and argyrodite. The mercury admixture varies from “not detected” in the central parts of grains to 0.22–1.70 wt % along the edges, or, in independent grains, to the appearance of Ag amalgams containing 10.20–24.61 wt % of Hg. The xenomorph form of grains of 50 μm or less in size prevails. It is assumed that the appearance of mercurial mineralization is caused by the superposition of products of the young Hg-bearing Dogda–Erikit belt upon the more ancient Ag-bearing Omsukchan trough.

AB - New data on mercurial mineralization are presented, and a detailed characteristic is given for the first discovery of mercurous silver in ores of the Rogovik gold–silver deposit (the Omsukchan trough, Northeastern Russia). It was found that native silver in the examined ores occurs as finely-dispersed inclusions in quartz filling microcracks and interstitions. It also occurs in associations with kustelite, Ag sulfosalts and selenides, selenitic acanthite, and argyrodite. The mercury admixture varies from “not detected” in the central parts of grains to 0.22–1.70 wt % along the edges, or, in independent grains, to the appearance of Ag amalgams containing 10.20–24.61 wt % of Hg. The xenomorph form of grains of 50 μm or less in size prevails. It is assumed that the appearance of mercurial mineralization is caused by the superposition of products of the young Hg-bearing Dogda–Erikit belt upon the more ancient Ag-bearing Omsukchan trough.

UR - http://www.scopus.com/inward/record.url?scp=85030676749&partnerID=8YFLogxK

U2 - 10.1134/S1028334X17090276

DO - 10.1134/S1028334X17090276

M3 - Article

AN - SCOPUS:85030676749

VL - 476

SP - 1094

EP - 1098

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 1

ER -

ID: 25728892